Abstract
The review considers bilateral interactions between bacteria and clay minerals and their influence on the chemical composition and chemical processes in soils. The participation of bacteria in the weathering, transformation and synthesis of new clay minerals is shown. These interactions contribute to changing the water-retaining properties of soils, ensuring their fertility, and contributes to the cycles of nutrients, inorganic and organic pollutants. Various processes of direct and indirect influence of phyllosilicates on microbiological activity and microbial diversity in soils and the possible biogeochemical role of these processes are described. Obviously, the prevalence of interaction types between bacteria and clay minerals is determined by the First Biogeochemical Principle formulated by V.I. Vernadsky
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.